{"data":{"id":"10.4121/85738a14-6652-4e0c-8552-d6fc729141b3","type":"dois","attributes":{"doi":"10.4121/85738a14-6652-4e0c-8552-d6fc729141b3","prefix":"10.4121","suffix":"85738a14-6652-4e0c-8552-d6fc729141b3","identifiers":[],"alternateIdentifiers":[],"creators":[{"name":"Haacker, Jan","nameType":"Personal","givenName":"Jan","familyName":"Haacker","nameIdentifiers":[{"nameIdentifier":"0000-0002-5464-2442","nameIdentifierScheme":"https://orcid.org/"}],"affiliation":[]},{"name":"Wouters, Bert","nameType":"Personal","givenName":"Bert","familyName":"Wouters","nameIdentifiers":[{"nameIdentifier":"0000-0002-1086-2435","nameIdentifierScheme":"https://orcid.org/"}],"affiliation":[]}],"titles":[{"title":"Glacier surface elevation change rate dataset accompanying the article \"CryoSwath: a CryoSat-2 swath processor and monthly surface elevation dataset for Arctic mountain glaciers\""}],"publisher":"4TU.ResearchData","container":{},"publicationYear":2026,"subjects":[{"subject":"Physical Geography and Environmental Geoscience","subjectScheme":"Australian and New Zealand Standard Research Classification (ANZSRC), 2008","classificationCode":"0406"},{"subject":"FOS: Earth and related environmental sciences","schemeUri":"http://www.oecd.org/science/inno/38235147.pdf","subjectScheme":"Fields of Science and Technology (FOS)"},{"subject":"Climate and Climate Change","subjectScheme":"Australian and New Zealand Standard Research Classification (ANZSRC), 2008","classificationCode":"9603"},{"subject":"Earth Sciences","subjectScheme":"Australian and New Zealand Standard Research Classification (ANZSRC), 2008","classificationCode":"04"},{"subject":"Environment","subjectScheme":"Australian and New Zealand Standard Research Classification (ANZSRC), 2008","classificationCode":"96"},{"subject":"Altimetry"},{"subject":"Arctic"},{"subject":"Climate change"},{"subject":"CryoSat"},{"subject":"glacier"},{"subject":"polar ice"},{"subject":"Remote Sensing"},{"subject":"Time: 2010-2024"}],"contributors":[{"name":"TU Delft, Faculty of Civil Engineering and Geosciences, Department of Geoscience and Remote Sensing","nameType":"Organizational","affiliation":[],"contributorType":"Other","nameIdentifiers":[]}],"dates":[{"date":"2026-06-12","dateType":"Issued"}],"language":"en","types":{"ris":"DATA","bibtex":"misc","citeproc":"dataset","schemaOrg":"Dataset","resourceType":"Dataset","resourceTypeGeneral":"Dataset"},"relatedIdentifiers":[{"relationType":"References","relatedIdentifier":"https://science-pds.cryosat.esa.int","relatedIdentifierType":"URL"},{"relationType":"References","relatedIdentifier":"https://doi.org/10.5281/zenodo.15064780","relatedIdentifierType":"URL"},{"relationType":"References","relatedIdentifier":"https://doi.org/10.4121/955d7f5a-0e3f-4166-a411-f0dcc4557cb2","relatedIdentifierType":"URL"},{"relationType":"References","relatedIdentifier":"https://github.com/j-haacker/cryoswath","relatedIdentifierType":"URL"},{"relationType":"IsVersionOf","relatedIdentifier":"10.4121/85738a14-6652-4e0c-8552-d6fc729141b3.v1","relatedIdentifierType":"DOI"},{"relationType":"IsVersionOf","relatedIdentifier":"10.4121/85738a14-6652-4e0c-8552-d6fc729141b3.v2","relatedIdentifierType":"DOI"},{"relationType":"IsVersionOf","relatedIdentifier":"10.4121/85738a14-6652-4e0c-8552-d6fc729141b3.v3","relatedIdentifierType":"DOI"},{"relationType":"IsVersionOf","relatedIdentifier":"10.4121/85738a14-6652-4e0c-8552-d6fc729141b3.v4","relatedIdentifierType":"DOI"}],"relatedItems":[],"sizes":[],"formats":["geospatial/netCDF4"],"version":"4","rightsList":[{"rights":"Creative Commons Attribution 4.0 International","rightsUri":"https://creativecommons.org/licenses/by/4.0/legalcode","schemeUri":"https://spdx.org/licenses/","rightsIdentifier":"cc-by-4.0","rightsIdentifierScheme":"SPDX"}],"descriptions":[{"description":"Most glaciers currently decline because of the rapid climate change. This dataset provides the glacier surface elevation change rates from radar altimetry presented in the accompanied article. The dataset includes all glaciers in the Arctic that are index in the Randolph Glacier Inventory (RGI) version 7.0. The data are derived from the European Space Agency's (ESA) mission CryoSat-2, which is best suited for glaciers covering several square kilometers. Where no observations were available we interpolated using statistical methods. The present dataset allows insights into dynamics of single glaciers, as well as into regional or Arctic-wide trends.\u003cbr\u003eThe source data were provided by the European Space Agency (ESA).This dataset was produced with CryoSwath 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